FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2012041811> ?p ?o ?g. }

• W2012041811 endingPage "n/a" @default.
• W2012041811 startingPage "n/a" @default.
• W2012041811 abstract "[1] Polarization and splitting analyses of minute-long windows of non-volcanic tremor at 3-component stations in the vicinity of southern Vancouver Island provide new evidence for the presence of anisotropy within the crustal portion of the North American plate beneath Cascadia. As reported previously, tremor particle motions are predominantly horizontal and inferred to manifest an upgoing wavefield composed primarily of S-waves. Under this assumption, estimates of incidence angle and back azimuth can be deduced from orientation of the smallest principle direction of motion. When subjected to standard S-wave splitting analysis, most stations yield systematic and reproducible fast polarization directions. Estimates of original polarization direction are more scattered and splitting times often exhibit multimodal distributions. Numerical simulations, wherein band-limited synthetic seismograms comprising contributions from multiple sources are analyzed for splitting, neatly reproduce these characteristics and thereby provide a framework for interpretation. A number of stations in our study sit astride the San Juan fault which, based on reflection studies, dips approximately 60 to 70° to the north. Underlying these stations is the Leech River Complex consisting of strongly foliated greenschist facies phyllites with steeply dipping foliations striking parallel to fast polarization directions of split S-waves. Detailed laboratory velocity measurements at elevated pressures show that as little as 2 to 3 km of vertically dipping Leech River phyllite are required to produce the observed splitting. These phyllites have some of the highest S-wave anisotropies measured to date and are part of a once continuous belt of anisotropic crust extending over 2000 km along the western North American coast from southern Vancouver Island to southwest Alaska." @default.
• W2012041811 created "2016-06-24" @default.
• W2012041811 creator A5005322254 @default.
• W2012041811 creator A5049809607 @default.
• W2012041811 date "2012-08-01" @default.
• W2012041811 modified "2023-10-01" @default.
• W2012041811 title "Split from slip and schist: Crustal anisotropy beneath northern Cascadia from non-volcanic tremor" @default.
• W2012041811 cites W1712686321 @default.
• W2012041811 cites W1967148892 @default.
• W2012041811 cites W1994004159 @default.
• W2012041811 cites W1997059152 @default.
• W2012041811 cites W2001820253 @default.
• W2012041811 cites W2011757749 @default.
• W2012041811 cites W2013028524 @default.
• W2012041811 cites W2014421120 @default.
• W2012041811 cites W2017662684 @default.
• W2012041811 cites W2022285033 @default.
• W2012041811 cites W2022585183 @default.
• W2012041811 cites W2030157739 @default.
• W2012041811 cites W2044123278 @default.
• W2012041811 cites W2047378493 @default.
• W2012041811 cites W2049589191 @default.
• W2012041811 cites W2054747879 @default.
• W2012041811 cites W2055972413 @default.
• W2012041811 cites W2066073101 @default.
• W2012041811 cites W2067488299 @default.
• W2012041811 cites W2074791332 @default.
• W2012041811 cites W2089371264 @default.
• W2012041811 cites W2095965656 @default.
• W2012041811 cites W2110362196 @default.
• W2012041811 cites W2119751136 @default.
• W2012041811 cites W2122927556 @default.
• W2012041811 cites W2125721743 @default.
• W2012041811 cites W2129057233 @default.
• W2012041811 cites W2132858240 @default.
• W2012041811 cites W2135916418 @default.
• W2012041811 cites W2139444382 @default.
• W2012041811 cites W2146909102 @default.
• W2012041811 cites W2161544177 @default.
• W2012041811 cites W2165524252 @default.
• W2012041811 cites W2166026905 @default.
• W2012041811 cites W2167380722 @default.
• W2012041811 cites W2187342034 @default.
• W2012041811 cites W2909239392 @default.
• W2012041811 doi "https://doi.org/10.1029/2011jb009095" @default.
• W2012041811 hasPublicationYear "2012" @default.
• W2012041811 type Work @default.
• W2012041811 sameAs 2012041811 @default.
• W2012041811 citedByCount "33" @default.
• W2012041811 countsByYear W20120418112012 @default.
• W2012041811 countsByYear W20120418112013 @default.
• W2012041811 countsByYear W20120418112014 @default.
• W2012041811 countsByYear W20120418112015 @default.
• W2012041811 countsByYear W20120418112016 @default.
• W2012041811 countsByYear W20120418112017 @default.
• W2012041811 countsByYear W20120418112018 @default.
• W2012041811 countsByYear W20120418112019 @default.
• W2012041811 countsByYear W20120418112020 @default.
• W2012041811 countsByYear W20120418112021 @default.
• W2012041811 countsByYear W20120418112022 @default.
• W2012041811 crossrefType "journal-article" @default.
• W2012041811 hasAuthorship W2012041811A5005322254 @default.
• W2012041811 hasAuthorship W2012041811A5049809607 @default.
• W2012041811 hasConcept C101139013 @default.
• W2012041811 hasConcept C120806208 @default.
• W2012041811 hasConcept C121332964 @default.
• W2012041811 hasConcept C127313418 @default.
• W2012041811 hasConcept C165205528 @default.
• W2012041811 hasConcept C195268267 @default.
• W2012041811 hasConcept C26687426 @default.
• W2012041811 hasConcept C58097730 @default.
• W2012041811 hasConcept C5900021 @default.
• W2012041811 hasConcept C62520636 @default.
• W2012041811 hasConcept C63441156 @default.
• W2012041811 hasConcept C77928131 @default.
• W2012041811 hasConcept C85725439 @default.
• W2012041811 hasConcept C97355855 @default.
• W2012041811 hasConceptScore W2012041811C101139013 @default.
• W2012041811 hasConceptScore W2012041811C120806208 @default.
• W2012041811 hasConceptScore W2012041811C121332964 @default.
• W2012041811 hasConceptScore W2012041811C127313418 @default.
• W2012041811 hasConceptScore W2012041811C165205528 @default.
• W2012041811 hasConceptScore W2012041811C195268267 @default.
• W2012041811 hasConceptScore W2012041811C26687426 @default.
• W2012041811 hasConceptScore W2012041811C58097730 @default.
• W2012041811 hasConceptScore W2012041811C5900021 @default.
• W2012041811 hasConceptScore W2012041811C62520636 @default.
• W2012041811 hasConceptScore W2012041811C63441156 @default.
• W2012041811 hasConceptScore W2012041811C77928131 @default.
• W2012041811 hasConceptScore W2012041811C85725439 @default.
• W2012041811 hasConceptScore W2012041811C97355855 @default.
• W2012041811 hasIssue "B8" @default.
• W2012041811 hasLocation W20120418111 @default.
• W2012041811 hasOpenAccess W2012041811 @default.
• W2012041811 hasPrimaryLocation W20120418111 @default.
• W2012041811 hasRelatedWork W1976229064 @default.
• W2012041811 hasRelatedWork W1999964904 @default.
• W2012041811 hasRelatedWork W2066073101 @default.

• next